X-ray photoelectron spectroscopic characterization of Silica Springs allophane

被引:12
作者
Childs, CW
Inoue, K
Seyama, H
Soma, M
Theng, BKG
Yuan, G
机构
[1] Victoria Univ Wellington, Sch Chem & Phys Sci, Wellington 1, New Zealand
[2] Iwate Univ, Fac Agr, Morioka, Iwate 020, Japan
[3] Natl Inst Environm Studies, Tsukuba, Ibaraki 305, Japan
[4] Manaaki Whenua Landcare Res, Palmerston North, New Zealand
关键词
D O I
10.1180/claymin.1997.032.4.07
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
A range of allophane samples (atomic Al/Si bulk ratios 1.1-1.9) from Silica Springs, New Zealand, has been characterized by X-ray photoelectron spectroscopy (XPS). Binding energies of Si 2s, Si 2p, Al 2p, O 1s, C Is, and N Is electrons, together with the kinetic energies of Al KL23L23 Auger electrons, at or near the surface of allophane aggregates, have been derived. The values for Al, Si and O electrons are similar to those for kaolinite but also to those for some framework silicates (feldspars) having 4-coordinate Al. Values for N electrons suggest that N occurs in organic structures. Comparison of XPS and bulk Al/Si ratios shows an enrichment of Al at or near the surface of allophane aggregates. The same is true for C and N. Extraction with citrate-dithionite-bicarbonate (CDB) reagent leaves the surfaces depleted in Al. The CDB extracts have higher Al/Si ratios than the bulk allophanes. Similarly, CDB treatment reduces the degree of surface enrichment of C and N. Small increases in the binding energies of Si electrons following CDB treatment suggest partial dissolution of the bulk structure though a concomitant removal of a separate phase or species cannot be ruled out. The results may be accounted for in terms of the structure previously suggested for the primary spherules of Silica Springs allophane (Childs et al., 1990) though the composition of the spherules at or near the surface of the allophane aggregates is different from those of the bulk.
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页码:565 / 572
页数:8
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